Thermokinetic Investigation of Binary Cu/Zn Hydroxycarbonates As Precursors for Cu/Zno Catalysts
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Evolution of Zincian Malachite Synthesis by Low Temperature Co
Evolution of zincian malachite synthesis by low temperature co- precipitation and its catalytic impact on the methanol synthesis Leon Zwienera, Frank Girgsdiesa, Daniel Brenneckea, Detre Teschnera,b, Albert G.F. Machokeb, Robert Schlögla,b, and Elias Frei*a [a] Department of Inorganic Chemistry, Fritz Haber Institute of the Max Planck Society, Faradayweg 4-6, 14195 Berlin, Germany. [b] Department of Heterogeneous Reactions, Max Planck Institute for Chemical Energy Conversion, Stiftstrasse 34 – 36, 45470 Mülheim an der Ruhr, Germany. *E-mail: [email protected] Keywords: zincian malachite • co-precipitation • methanol synthesis Abstract: Low temperature co-precipitation enabled, for the first time, the preparation of phase pure zincian malachite precursors with Zn contents of up to 31 at.-%. The high Zn content was beneficial for maximizing the dispersion of Cu and oxygen defect sites on the ZnO surface. Further, an increase of the Zn loading from 10 to 31 at.-% doubled the specific surface areas obtained from N2O-RFC (Reactive Frontal Chromatography) and H2- TA (Transient Adsorption). As the Zn content was increased from 10 to 31 at.-%, the apparent activation energy for methanol formation was strongly decreased. Furthermore, water formation was reduced indicating a retardation of the rWGS in favor of methanol formation at high Zn loadings. Additionally, compared to high temperature co-precipitation, low temperature precipitated catalysts exhibited increased catalytic activities. 1. Introduction Rising global energy demand, relying on the ongoing consumption of fossil fuels, has led to a drastic increase in atmospheric CO2 concentration over the past century.[1] Since CO2 has been attributed to be the main anthropogenic source of the greenhouse effect, CO2 has become a valuable carbon source available for chemical conversion (e.g. -
Aurichalcite (Zn, Cu)5(CO3)2(OH)6 C 2001-2005 Mineral Data Publishing, Version 1
Aurichalcite (Zn, Cu)5(CO3)2(OH)6 c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Monoclinic, pseudo-orthorhombic by twinning. Point Group: 2/m. As acicular to lathlike crystals with prominent {010}, commonly striated k [001], with wedgelike terminations, to 3 cm. Typically in tufted divergent sprays or spherical aggregates, may be in thick crusts; rarely columnar, laminated or granular. Twinning: Observed in X-ray patterns. Physical Properties: Cleavage: On {010} and {100}, perfect. Tenacity: “Fragile”. Hardness = 1–2 D(meas.) = 3.96 D(calc.) = 3.93–3.94 Optical Properties: Transparent to translucent. Color: Pale green, greenish blue, sky-blue; colorless to pale blue, pale green in transmitted light. Luster: Silky to pearly. Optical Class: Biaxial (–). Pleochroism: Weak; X = colorless; Y = Z = blue-green. Orientation: X = b; Y ' a; Z ' c. Dispersion: r< v; strong. α = 1.654–1.661 β = 1.740–1.749 γ = 1.743–1.756 2V(meas.) = Very small. Cell Data: Space Group: P 21/m. a = 13.82(2) b = 6.419(3) c = 5.29(3) β = 101.04(2)◦ Z=2 X-ray Powder Pattern: Mapim´ı,Mexico. 6.78 (10), 2.61 (8), 3.68 (7), 2.89 (4), 2.72 (4), 1.827 (4), 1.656 (4) Chemistry: (1) CO2 16.22 CuO 19.87 ZnO 54.01 CaO 0.36 H2O 9.93 Total 100.39 (1) Utah; corresponds to (Zn3.63Cu1.37)Σ=5.00(CO3)2(OH)6. Occurrence: In the oxidized zones of copper and zinc deposits. Association: Rosasite, smithsonite, hemimorphite, hydrozincite, malachite, azurite. -
Infrare D Transmission Spectra of Carbonate Minerals
Infrare d Transmission Spectra of Carbonate Mineral s THE NATURAL HISTORY MUSEUM Infrare d Transmission Spectra of Carbonate Mineral s G. C. Jones Department of Mineralogy The Natural History Museum London, UK and B. Jackson Department of Geology Royal Museum of Scotland Edinburgh, UK A collaborative project of The Natural History Museum and National Museums of Scotland E3 SPRINGER-SCIENCE+BUSINESS MEDIA, B.V. Firs t editio n 1 993 © 1993 Springer Science+Business Media Dordrecht Originally published by Chapman & Hall in 1993 Softcover reprint of the hardcover 1st edition 1993 Typese t at the Natura l Histor y Museu m ISBN 978-94-010-4940-5 ISBN 978-94-011-2120-0 (eBook) DOI 10.1007/978-94-011-2120-0 Apar t fro m any fair dealin g for the purpose s of researc h or privat e study , or criticis m or review , as permitte d unde r the UK Copyrigh t Design s and Patent s Act , 1988, thi s publicatio n may not be reproduced , stored , or transmitted , in any for m or by any means , withou t the prio r permissio n in writin g of the publishers , or in the case of reprographi c reproductio n onl y in accordanc e wit h the term s of the licence s issue d by the Copyrigh t Licensin g Agenc y in the UK, or in accordanc e wit h the term s of licence s issue d by the appropriat e Reproductio n Right s Organizatio n outsid e the UK. Enquirie s concernin g reproductio n outsid e the term s state d here shoul d be sent to the publisher s at the Londo n addres s printe d on thi s page. -
Download PDF About Minerals Sorted by Mineral Group
MINERALS SORTED BY MINERAL GROUP Most minerals are chemically classified as native elements, sulfides, sulfates, oxides, silicates, carbonates, phosphates, halides, nitrates, tungstates, molybdates, arsenates, or vanadates. More information on and photographs of these minerals in Kentucky is available in the book “Rocks and Minerals of Kentucky” (Anderson, 1994). NATIVE ELEMENTS (DIAMOND, SULFUR, GOLD) Native elements are minerals composed of only one element, such as copper, sulfur, gold, silver, and diamond. They are not common in Kentucky, but are mentioned because of their appeal to collectors. DIAMOND Crystal system: isometric. Cleavage: perfect octahedral. Color: colorless, pale shades of yellow, orange, or blue. Hardness: 10. Specific gravity: 3.5. Uses: jewelry, saws, polishing equipment. Diamond, the hardest of any naturally formed mineral, is also highly refractive, causing light to be split into a spectrum of colors commonly called play of colors. Because of its high specific gravity, it is easily concentrated in alluvial gravels, where it can be mined. This is one of the main mining methods used in South Africa, where most of the world's diamonds originate. The source rock of diamonds is the igneous rock kimberlite, also referred to as diamond pipe. A nongem variety of diamond is called bort. Kentucky has kimberlites in Elliott County in eastern Kentucky and Crittenden and Livingston Counties in western Kentucky, but no diamonds have ever been discovered in or authenticated from these rocks. A diamond was found in Adair County, but it was determined to have been brought in from somewhere else. SULFUR Crystal system: orthorhombic. Fracture: uneven. Color: yellow. Hardness 1 to 2. -
The Oxidized Zinc Ores of Leadville Colorado
DEPARTMENT OF THE INTERIOR FRANKLIN K. LANE, Secretary / ? */ 2~ J o UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, Director Bulletin 681 THE OXIDIZED ZINC ORES OF LEADVILLE COLORADO BY G. F. LOUGHLIN WASHINGTON GOVERNMENT PRINTING OFFICE 1918 *? o o CONTENTS. Page- Introduction. ............................................................. 7 Discovery.....................................................'............ 7 Early accounts of zinc carbonate and silicate............................. 8 Recent discovery of oxidized zinc ore bodies............................. 12 Production................................................................ 13 Literature.................................................................. 16 Mineralogy................................................................... 17 Zinc-ore minerals....................................................... 17 Smithsonite....................................................... 17 Hydrozincite....................................................... 18 Aurichalcite..................................'..................... 19 Calamine......................................................... 20 Hetaerolite....................................................... 21 Chalcophanite..................................................... 24 Zinciferous clay................................................... 24 Deschenite........................................................ 28 Associated minerals.................................................... 28 Iron oxides....................................................... -
Minerals of Arizona Report
MINERALS OF ARIZONA by Frederic W. Galbraith and Daniel J. Brennan THE ARIZONA BUREAU OF MINES Price One Dollar Free to Residents of Arizona Bulletin 181 1970 THE UNIVERSITY OF ARIZONA TUCSON TABLE OF CONT'ENTS EIements .___ 1 FOREWORD Sulfides ._______________________ 9 As a service about mineral matters in Arizona, the Arizona Bureau Sulfosalts ._. .___ __ 22 of Mines, University of Arizona, is pleased to reprint the long-standing booklet on MINERALS OF ARIZONA. This basic journal was issued originally in 1941, under the authorship of Dr. Frederic W. Galbraith, as Simple Oxides .. 26 a bulletin of the Arizona Bureau of Mines. It has moved through several editions and, in some later printings, it was authored jointly by Dr. Gal Oxides Containing Uranium, Thorium, Zirconium .. .... 34 braith and Dr. Daniel J. Brennan. It now is being released in its Fourth Edition as Bulletin 181, Arizona Bureau of Mines. Hydroxides .. .. 35 The comprehensive coverage of mineral information contained in the bulletin should serve to give notable and continuing benefits to laymen as well as to professional scientists of Arizona. Multiple Oxides 37 J. D. Forrester, Director Arizona Bureau of Mines Multiple Oxides Containing Columbium, February 2, 1970 Tantaum, Titanium .. .. .. 40 Halides .. .. __ ____ _________ __ __ 41 Carbonates, Nitrates, Borates .. .... .. 45 Sulfates, Chromates, Tellurites .. .. .. __ .._.. __ 57 Phosphates, Arsenates, Vanadates, Antimonates .._ 68 First Edition (Bulletin 149) July 1, 1941 Vanadium Oxysalts ...... .......... 76 Second Edition, Revised (Bulletin 153) April, 1947 Third Edition, Revised 1959; Second Printing 1966 Fourth Edition (Bulletin 181) February, 1970 Tungstates, Molybdates.. _. .. .. .. 79 Silicates ... -
Oxidized Zinc Deposits of the United States
Oxidized Zinc Deposits of the United States GEOLOGICAL SURVEY BULLETIN 1135 This bulletin was published as separate chapters A-C UNITED STATES DEPARTMENT--OF THE INTERIOR STEWART· L.' ·UDALL,. Secretary - GEOLOGICAL SURVEY Thomas B. Nolan, Director CONTENTS [The letters in parentheses preceding the titles designate separately published chapters] Oxidized zinc deposits of the United States: (A) Part 1. General geology. (B) Part 2. Utah. ( 0) Part 3. Colorado. 0 Oxidized Zinc Deposits of the United States Part 1. General Geology By ALLEN V. HEYL and C. N. BOZION GEOLOGICAL SURVEY BULLETIN 1135-A Descriptions of the many varieties of ox idized zinc deposits of supergeneland hypogene origin UNITED STATES GOVERNMENT PRINTING OFFICE1 WASHINGTON a 1962 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington 25, D.C. CONTENTS Page Abstract---------------------------------------------------------- A-1 Introduction------------------------------------------------------ 1 Distribution_ _ _ _ __ _ _ _ _ _ __ __ _ __ _ _ _ _ _ _ _ __ __ __ __ __ _ _ _ __ _ __ _ _ _ _ _ __ __ _ _ 3 Mliner&ogY------------------------------------------------------- 5 Commercial ores___________________________________________________ 7 Varieties----------------------------------------------------- 7 Grades------------------------------------------------------- 9 Generalgeology___________________________________________________ -
Plattnerite Pbo2 C 2001-2005 Mineral Data Publishing, Version 1 Crystal Data: Tetragonal
Plattnerite PbO2 c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Tetragonal. Point Group: 4/m 2/m 2/m. Commonly as crystals, prismatic k [001], showing {010}, {011}, {110}, {131}, {001}, to 5 mm; may be nodular or botryoidal, fibrous and concentrically zoned, massive. Twinning: On {011}, as contact and penetration twins, rarely polysynthetic. Physical Properties: Tenacity: Brittle. Hardness = 5.5 D(meas.) = 9.564 D(calc.) = 9.563 Optical Properties: Opaque to slightly translucent. Color: Jet-black, iron-black, brownish black; yellowish in transmitted light; gray-white in reflected light, with red-brown internal reflections. Streak: Chestnut-brown. Luster: Bright metallic to adamantine; tarnishing dull on exposure. Optical Class: Uniaxial. Pleochroism: Distinct. n = 2.30(5) Anisotropism: Noticeable; midnight-blue. R1–R2: (400) 18.5–21.3, (420) 18.4–21.9, (440) 18.5–21.5, (460) 18.5–20.2, (480) 18.5–19.8, (500) 18.4–19.4, (520) 18.2–18.9, (540) 17.9–18.4, (560) 17.5–18.0, (580) 17.0–17.4, (600) 16.5–16.9, (620) 16.0–16.4, (640) 15.5–15.9, (660) 15.0–15.4, (680) 14.4–15.0, (700) 14.0–14.5 Cell Data: Space Group: P 42/mnm. a = 4.9525(4) c = 3.3863(4) Z = 2 X-ray Powder Pattern: Ojuela mine, Mexico. 3.500 (100), 2.793 (94), 1.855 (80), 2.469 (40), 1.524 (23), 0.823 (20), 1.568 (19) Chemistry: (1) PbO2 99.6 CuO 0.1 Total 99.7 (1) Ojuela mine, Mexico; by electron microprobe. -
Rosasite (Cu, Zn)2(CO3)(OH)2 C 2001-2005 Mineral Data Publishing, Version 1
Rosasite (Cu, Zn)2(CO3)(OH)2 c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Monoclinic. Point Group: 2/m. Crystals are acicular, to 0.5 mm; in radial or divergent sprays or globular; compact mammillary to botryoidal crusts and masses, typically fibrous and with warty surfaces. Twinning: On {100}. Physical Properties: Cleavage: In two directions. Tenacity: Brittle. Hardness = 4.5 D(meas.) = 4.0–4.2 D(calc.) = 4.15 Optical Properties: Semitransparent. Color: Green, bluish green, sky-blue; pale blue to colorless in transmitted light. Optical Class: Biaxial (–). Pleochroism: Strong; X = pale emerald-green; Z = dark emerald-green. Orientation: X = c; Y ∧ a ' 10◦. Absorption: X > Y > Z. α = 1.672–1.688 β = 1.796–1.83 γ = 1.811–1.831 2V(meas.) = 33(5)◦ 2V(calc.) = 36.4◦ Cell Data: Space Group: P 21/a. a = 12.873(3) b = 9.354(3) c = 3.156(2) β = 110.36(3)◦ Z=4 X-ray Powder Pattern: Tsumeb, Namibia. 2.600 (100), 6.05 (90), 5.07 (90), 3.69 (90), 2.962 (70), 2.534 (50), 2.144 (50) Chemistry: (1) (2) CO2 19.54 19.74 CuO 47.53 35.68 ZnO 24.60 36.50 H2O 8.33 8.08 Total [100.00] 100.00 (1) Sardinia; recalculated to 100% from an original total of 100.37% after deduction of MgO 0.15%, Fe2O3 0.39%, insoluble 0.33%. (2) (Cu, Zn)2(CO3)(OH)2 with Cu:Zn = 1:1. Mineral Group: Rosasite group. Occurrence: An uncommon secondary mineral in the oxidized zone of Cu–Zn-bearing deposits, typically formed by zinc-bearing solutions on primary copper minerals; may be of post-mine origin. -
THE MINERALOGY of the Mapiml' MINING DISTRICT, DURANGO
The mineralogy of the Mapimí mining district, Durango, Mexico Item Type text; Dissertation-Reproduction (electronic) Authors Hoffmann, Victor Joseph 1935- Publisher The University of Arizona. Rights Copyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author. Download date 05/10/2021 08:35:35 Link to Item http://hdl.handle.net/10150/565169 THE MINERALOGY OF THE MAPIMl' MINING DISTRICT, DURANGO, MEXICO by Victor Joseph Hoffmann A Dissertation Submitted to the Faculty of the DEPARTMENT OF GEOLOGY In Partial Fulfillment of the Requirements For the Degree of DOCTOR OF PHILOSOPHY In the Graduate College THE UNIVERSITY OF ARIZONA 19 6 8 THE UNIVERSITY OF ARIZONA GRADUATE COLLEGE I hereby recommend that this dissertation prepared under my direction by _________ Victor Joseph Hoffmann____________________ entitled The Mineralogy of the Mapimi Mining District,______ Durango, Mexico______________________________ be accepted as fulfilling the dissertation requirement of the degree of Doctor of Philosophy_______________________________ ____________ ‘7/2 __________________ Dissertation Director^/ Date z / ~ After inspection of the final copy of the dissertation, the following members of the Final Examination Committee concur in its approval and recommend its acceptance:* f , A> Q ~/ w n n rT 2.7, 7 / f / 7 u Z Z /9<$7 •fs---------- - ' -------7 This approval and acceptance is contingent on the candidate's adequate performance and defense of this dissertation at the final oral examination. The inclusion of this sheet bound into the library copy of the dissertation is evidence of satisfactory performance at the final examination. -
The Microscopic Determination of the Nonopaque Minerals
DEPARTMENT OF THE INTERIOR ALBERT B. FALL, Secretary UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, Director Bulletin 679 THE MICROSCOPIC DETERMINATION OF THE NONOPAQUE MINERALS BY ESPER S. LARSEN WASHINGTON GOVERNMENT PRINTING OFFICE 1921 CONTENTS. CHAPTER I. Introduction.................................................. 5 The immersion method of identifying minerals........................... 5 New data............................................................. 5 Need of further data.................................................... 6 Advantages of the immersion method.................................... 6 Other suggested uses for the method.................................... 7 Work and acknowledgments............................................. 7 CHAPTER II. Methods of determining the optical constants of minerals ....... 9 The chief optical constants and their interrelations....................... 9 Measurement of indices of refraction.................................... 12 The embedding method............................................ 12 The method of oblique illumination............................. 13 The method of central illumination.............................. 14 Immersion media.................................................. 14 General features............................................... 14 Piperine and iodides............................................ 16 Sulphur-selenium melts....................................... 38 Selenium and arsenic selenide melts........................... 20 Methods of standardizing -
SOME NEW OCCURRENCES of MINERALS of ARIZONA B Y
53 SOME NEW OCCURREN CES OF MINERALS OF ARIZONA B y Ri c hard A. Bideaux a nd Sidney A. Willia m s Department of Geology, Uni v ersity of Arizo n a and Richard W. T homssen The Anaconda Company The following list is a c ompilation of rec ently rec ognized mineral o ccurrences whic h are not included in Minerals of A r izona (1). Thir t y -thr e e specie s prev iously unreported in Arizona hav e b e en a d ded; the se are indic ated b y a n asterisk. After each occurrence the identifier, discov erer, or j>rincipal referent is indicated in parentheses. * Aegirine-aug ite --with sphene, scapolite and other spe cies listed below in a pulaskite-melatutv etite dike; Gunsig ht Mtn. , N. end of Sierrita Mtns., Pima Co. (SAW, R WT) * Aeg irine - -in a pulaskite dik e ; Gunsig ht Mtn. , Pima C o . (SAW, R WT) * Aerinite --in a pulaskite dike; Gunsig ht Mtn., Pima C o . (SAW, R WT) Allanite - -with e pidote, actinolite and apatite; Lin da Lee claim, Quijotoa Mtns ., Pima Co. (SAW) Andalusite --v ar. titanandalusite w ith sillimanite, corundum and c ordierite; Gila Riv er Indian Reserv ation, 10 miles N. of Casa Grande, Pinal Co. (SAW) Anglesite --large orebody; some specimens showing relic galena; Glov e mine, Santa Rita Mtns., Santa Cruz Co. (RAB) * Apophyllite --as subhedral grains with v esuvianite &: wollastonite in tactite; T o mbstone, Cochise Co. (SAW) Atac amite --as laths in c hry socolla and cornuite (var.